Application of nuclear microprobe to the study of metasomatism in mantle peridotites | |
Chen, YH; Zhu, JQ; Lu, RG; Wu, XK; Gu, YM; Li, XL; Zhang, Q | |
刊名 | NUCLEAR INSTRUMENTS & METHODS IN PHYSICS RESEARCH SECTION B-BEAM INTERACTIONS WITH MATERIALS AND ATOMS |
1997-07-01 | |
卷号 | 130期号:1-4页码:700-705 |
ISSN号 | 0168-583X |
文献子类 | Article |
英文摘要 | In recent years, some models have been proposed to explain the chemical heterogeneity of the earth mantle. Among them the metasomatism by the mantle fluid and the mantle melt is the most popular one. The trace elemental behavior of the mantle minerals from different areas in micron scales can provide important information on the understanding of the mantle metasomatism. This paper describes the study of the metasomatism in mantle peridotites from Raobazhai, Anhui Province of China by the nuclear microprobe. The concentrations and distributions of trace elements in the metasomatized mantle peridotite were determined quantitatively by the micro-PIXE software package TTSPM. The internal standard and the integrated iterative method were used for the calculation. The matrix elements in the minerals were analyzed by EPMA. The accuracy of the quantitative analysis was examined by three geochemical standards of rocks (GSR). The results were better than 15% for most elements. According to the elemental maps, the trace element distributions in the amphibole, which was crystallized from the mantle fluid, displayed obvious heterogeneity and zoning. The enrichment of Ni, Zn, Ga, Rb, Sr, Y, Zr and Pb in the mineral could be associated with the metasomatism of the mantle fluid. The local coexistence of Ni, Cu, Pb, Ee and S in the amphibole suggested that there were xenoliths trapped in the minerals during their crystallization. The characteristics of the trace element composition and distribution in the mantle peridotites demonstrated that the metasomatism by the mantle fluid and the mantle melt might change the chemical composition of the mantle peridotites and thus resulted in the chemical heterogeneity of the earth mantle. (C) 1997 Elsevier Science B.V. |
WOS关键词 | SYSTEM |
WOS研究方向 | Instruments & Instrumentation ; Nuclear Science & Technology ; Physics |
语种 | 英语 |
出版者 | ELSEVIER SCIENCE BV |
WOS记录号 | WOS:A1997XZ01700118 |
内容类型 | 期刊论文 |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/82012] |
专题 | 中国科学院地质与地球物理研究所 |
作者单位 | 1.CHINESE ACAD SCI,SHANGHAI INST NUCL RES,SHANGHAI 201800,PEOPLES R CHINA 2.CHINESE ACAD SCI,INST GEOL,BEIJING 100029,PEOPLES R CHINA |
推荐引用方式 GB/T 7714 | Chen, YH,Zhu, JQ,Lu, RG,et al. Application of nuclear microprobe to the study of metasomatism in mantle peridotites[J]. NUCLEAR INSTRUMENTS & METHODS IN PHYSICS RESEARCH SECTION B-BEAM INTERACTIONS WITH MATERIALS AND ATOMS,1997,130(1-4):700-705. |
APA | Chen, YH.,Zhu, JQ.,Lu, RG.,Wu, XK.,Gu, YM.,...&Zhang, Q.(1997).Application of nuclear microprobe to the study of metasomatism in mantle peridotites.NUCLEAR INSTRUMENTS & METHODS IN PHYSICS RESEARCH SECTION B-BEAM INTERACTIONS WITH MATERIALS AND ATOMS,130(1-4),700-705. |
MLA | Chen, YH,et al."Application of nuclear microprobe to the study of metasomatism in mantle peridotites".NUCLEAR INSTRUMENTS & METHODS IN PHYSICS RESEARCH SECTION B-BEAM INTERACTIONS WITH MATERIALS AND ATOMS 130.1-4(1997):700-705. |
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